The flow of time in the Connecticut valley : $b geological imprintsBain, George W. (George William)
Science
The flow of time in the Connecticut valley : $b geological imprints
Bain, George W. (George William)
Geology -- Connecticut River Valley
Route 32 from Petersham and Worcester enters from the left (22.7) just
before the highway dips into the creek bottom at the edge of the Quabbin
basin. Thence it ascends to the New England upland level, where a
lookout (25.5) affords an expansive view to the east and north, with
Mount Monadnock rising prominently on the distant skyline. New Salem
(25.8) is on the hilltop. Hornblende schist outcrops at intervals across
the broad ridge, and especially near the descent (28.4) southwestward to
another stream (30.3) which empties into the Quabbin Reservoir. Once
again the highway climbs rather steadily for three and one-half miles,
passing the Shutesbury road (31.0) on the right, until it reaches
another lookout (34.6) from which the trenched New England upland
spreads out to the east. Pelham gneiss is the main rock on the broad
ridge west of the Quabbin basin, especially in the vicinity of Pelham
(35.2), which gave the rock its name.
The tour turns east to Amherst (41.7), following a section which has
been described elsewhere (see pp. 78-79). The principal sights include
the panorama of the Connecticut Lowland and the ice-margin lake
deposits. The drive from Amherst to Northampton (see pp. 78-79) and from
Northampton to South Deerfield (see pp. 87-88) on Federal Highway 5 has
likewise been covered in other tours, but some new features may be seen
along the shorter route from Amherst to Sunderland.
The Sunderland road turns right at the north end of the Amherst common.
It descends, first, from Amherst Island, in glacial Lake Hadley, to the
old beach at Massachusetts State College (42.6), and then from the beach
to the lake bottom (43.2) north of the campus. The route takes the left
fork in North Amherst (44.2), traverses part of the old lake bed, swings
west around the Long Plain delta (45.5), and crosses its entrenched
brook (46.1). Most of the stream’s water seeps through the delta sands
and gravels, and emerges in springs at the Fish Hatchery (46.3). Gravel
pits across the road furnish an excellent section of the fore-set and
top-set beds of the delta. The road right (46.8) goes to the delta top
east of Mount Toby, Montague and Turners Falls, but the main highway
continues north.
Public-domain text, read in full here on John Shaqi.
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